Earthquakes
Earthquakes
The Andes mountains were formed from the interaction of the South American Plate and the Nazca Plate, which is a convergent plate boundary. The Nazca Plate is subducting beneath the South American Plate, leading to the uplift and formation of the Andes mountains.
The Andes Mountain Chain is formed as a result of a convergent plate boundary, the collision of the South American Plate with the Nazca Plate.
Hello! The answer is the Nazca Plate and the South American Plate. The Nazca Plate is sub-ducting (going down) the South American Plate. That is how the Andes are being formed.
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.
The Andes mountain range is being formed by the convergence of the Nazca and South American plates. This process involves the oceanic Nazca Plate subducting beneath the South American Plate, leading to the uplift of the Andes mountains.
The East Pacific Rise separates the Nazca Plate from the Pacific Plate.
At the western edge of the Nazca plate and the eastern edge of the Pacific plate lies the East Pacific Rise. The East Pacific Rice is known as a mid-ocean ridge, formed from a divergent boundary.
The Nazca plate shares both convergent and divergent boundaries. The Pacific plate has both a transform boundary and divergent boundary
Examples of collision mountain ranges include the Himalayas (formed by the collision of the Indian Plate with the Eurasian Plate), the Alps (formed by the collision of the African Plate with the Eurasian Plate), and the Andes (formed by the collision of the South American Plate with the Nazca Plate).
nazca plate
When the Nazca Plate pushes into the South American Plate, it creates a convergent boundary. This leads to subduction, where the denser Nazca Plate is forced beneath the South American Plate. This process can result in the formation of volcanic arcs and earthquakes along the boundary.